Water and moganite participation in agates from Bou Hamza (Morocco). [PDF]
Powolny T +3 more
europepmc +1 more source
Spatial ecology of moose in Sweden: Combined Sr-O-C isotope analyses of bone and antler. [PDF]
Armaroli E +3 more
europepmc +1 more source
Geochemistry of metabasites in the Variscan basement of NE Sardinia, Italy
Utzeri D. +3 more
core
A rapid transition from subduction to Barrovian metamorphism: geochronology of mafic-ultramafic relicts of oceanic crust in the Central Alps, Switzerland. [PDF]
Lemke K, Rubatto D, Hermann J.
europepmc +1 more source
The myth of the De Geer Zone: a change of paradigm for the opening of the Fram Strait. [PDF]
Koehl JP.
europepmc +1 more source
Geochemical data of Al-rich diopside pyroxenites from the Premosello mantle peridotite massif, Ivrea-Verbano Zone, Southern Alps. [PDF]
Ogunyele AC +4 more
europepmc +1 more source
Migmatites and partial melting in the Variscan chain of NE Sardinia, Italy
Utzeri D. +3 more
core
Carboniferous: oblique-slip basins, intraplate magmatism and the Variscan Orogeny
Monaghan, Alison A. +4 more
openaire +1 more source
Related searches:
Two plates — Many subduction zones: The Variscan orogeny reconsidered
Gondwana Research, 2013Abstract The Variscides of Europe and N-Africa are the result of the convergence of the plates of Gondwana and Laurussia in the Paleozoic. This orogen is characterized by the juxtaposition of blocks of continental crust that are little affected by the Variscan orogeny.
R L Romer
exaly +5 more sources
Variscan orogeny in the Black Sea region
International Journal of Earth Sciences, 2016Two Gondwana-derived Paleozoic belts rim the Archean/Paleoproterozoic nucleus of the East European Platform in the Black Sea region. In the north is a belt of Paleozoic passive-margin-type sedimentary rocks, which extends from Moesia to the Istanbul Zone and to parts of the Scythian Platform (the MOIS Block).
Aral I. Okay, Gültekin Topuz
openaire +1 more source

